Hostname: page-component-848d4c4894-75dct Total loading time: 0 Render date: 2024-06-05T08:34:01.421Z Has data issue: false hasContentIssue false

Current Directions from Folded Strata

Published online by Cambridge University Press:  01 May 2009

W. A. Cummins
Affiliation:
Department of Geology, The University, Nottingham.

Abstract

In current direction studies, when unfolding strata to their original horizontal attitude, plunge is usually allowed for on the assumption that it was acquired by rotation about horizontal axis at right-angles to the fold axis. Errors resulting from plunge correction on this assumption, if mistaken, are examined

Type
Articles
Copyright
Copyright © Cambridge University Press 1964

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Craig, G. Y., and Walton, E. K., 1962. Sedimentary Structures and Palaeo-current Directions from the Silurian Rocks of Kirkcudbrightshire. Trans. Edin. geol. Soc., 19, 100.CrossRefGoogle Scholar
Cummins, W. A., 1957. The Denbigh Grits; Wenlock Greywackes in Wales. Geol. Mag., 94, 433.CrossRefGoogle Scholar
Haaf, E. Ten, 1959. Graded Beds of the Northern Apennines. Ph.D. Thesis. Groningen.Google Scholar
Norman, T. N., 1960. Azimuths of Primary Linear Structures in Folded Strata. Geol. Mag., 97, 338.CrossRefGoogle Scholar
Ramsay, J. G., 1961. The Effects of Folding on the Orientation of Sedimentation Structures. J. Geol., 69, 84.CrossRefGoogle Scholar